泸州X波段双偏振雷达在冰雹识别中的对比应用

Application of X-Band Dual-Polarization Radar in Hail Recognition in Luzhou

  • 摘要: 利用实况观测资料、714X波段双偏振多普勒雷达和5部拼接的S波段雷达资料,对2020年5月30日泸州一次冰雹过程进行对比分析。结果表明:此次冰雹过程是在200hPa西风急流、850hPa切变、地面辐合线和冷空气的共同作用下发生的。整层大气具有强的不稳定性,存在较强的风切变,各项探空指数也有利于冰雹等强对流天气的发生。冰雹过程中,X波段的回波位置和实际降水、降雹区相匹配,但回波强度偏弱;S波段的回波位置较实况落区偏西,回波强度和实况更匹配。S波段的VIL能够较好地反应冰雹粒子的存在。X波段的RHV能够有效地区分冰雹和强降水回波,而KDP、ZDR存在空洞现象,应用稳定性较差,需结合其它参量进行冰雹识别。

     

    Abstract: A hail process in Luzhou on May 30, 2020 was compared and analyzed by using the actual observation data, 714X-band dual polarization Doppler radar data and five splicing S-band radar data. The main conclusions are as following: The hail process occurred under the joint action of 200hPa westerly jet, 850hPa shear, ground convergence line and cold air. The whole atmosphere has strong instability, strong wind shear, and various sounding indexes are also conducive to the occurrence of severe convective weather such as hail. In the process, the echo position of X band matches the actual precipitation and hail area, but the echo intensity is weak. The echo position of S band is wester than the actual area, and the echo intensity matches the actual situation better. S-band VIL can better reflect the presence of hail particles. The X-band RHV can effectively distinguish hail and heavy rainfall echo, while the KDP and ZDR have holes, and the application stability is poor, it is necessary to combine other parameters to identify hail.

     

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